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Niagara, Wisconsin

Well Drillers Near Niagara, Wisconsin

Typical Niagara area geology: surficial sand/gravel overlying granite bedrock. Residential wells typically reach granite at 20–45 ft, with wells drilled 100–225+ ft for consistent supply.

Showing contractors within 60 miles of Niagara. 11 results found.

Typical depth
140 ft
Water table
21 ft
Contractors
11

11 Contractors

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Kleiman Pump & Well Drilling Inc logo

Kleiman Pump & Well Drilling Inc

Active Driller
Iron Mountain, MI 49801-0704
Well DrillingPump ServicesPump Installation+6 more
Morin & Johnson Well Drilling & Pump Inc logo

Morin & Johnson Well Drilling & Pump Inc

NIAGRA, WI 54151-
Well DrillingCable ToolPump Services+2 more

Romitti Well Drilling & Pumps

Niagara, WI 54151
Well DrillingWell MaintenanceFiltration

Boussum Well Drilling Inc

Active Driller
Channing, MI 49815
Well DrillingPump InstallationWell Maintenance

Kozikowski Well & Pump, Inc.

Active Driller
Menominee, MI 49858-9699
Well DrillingPump ServicesPump Installation+1 more

North Tech Pump Installing

Crivitz, WI 54114
Complete SystemsWater System Maintenance
t and t Well Drilling llc logo

t and t Well Drilling llc

Lakewood, WI 54138
Well DrillingPump Services
Hakala Well & Pump Services logo

Hakala Well & Pump Services

Active Driller
Negaunee, MI 49866
Pump InstallationPump RepairWell Maintenance+1 more

Webster Well Drilling

Negaunee, MI 49866
Well DrillingResidential Well DrillingComplete Water System Installation

Howard's Water Pumps & Services

Escanaba, MI 49829
Pump InstallationPump Repair

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View Local Geology Report

A geological estimate for the Niagara area.

Typical Well Depth
140 ft
Static Water Level
21 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

In the Niagara, WI region, well logs consistently show an upper sequence of unconsolidated sand and gravel ranging from about 8 to 72 feet, commonly 20–45 feet thick. This is typically underlain by granite or hard rock, which forms the primary aquifer below these unconsolidated deposits. Wells for residential use (5–15+ GPM) are generally cased through the sand/gravel into or just past the granite, seldom exceeding 150–225 feet total depth. High-capacity or low-yield sites may go deeper into the granite. Casing is usually set at the base of the unconsolidated material (35–45 ft). Static water levels are generally 18–25 ft below ground surface, and rotary mud circulation is the dominant drilling method. Grout is primarily cement, sealing surface to casing depth.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
035 ftSand and GravelUnconsolidated sand (often with gravel/cobble, sometimes clay or silt interbeds); typically yellow/dirty to clean, soft-caving.Color: Yellow, grey, or dirty
Hardness: Soft
35145 ftGranite/Hard RockCrystalline granite or very hard bedrock; major aquifer zone for most wells.Color: Grey or black
Hardness: Hard

Frequently Asked Questions

A typical residential well in the Niagara area is drilled to approximately 140 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 21 feet below the surface in this region.

In the Niagara, WI region, well logs consistently show an upper sequence of unconsolidated sand and gravel ranging from about 8 to 72 feet, commonly 20–45 feet thick. This is typically underlain by granite or hard rock, which forms the primary aquifer below these unconsolidated deposits. Wells for residential use (5–15+ GPM) are generally cased through the sand/gravel into or just past the granite, seldom exceeding 150–225 feet total depth. High-capacity or low-yield sites may go deeper into the granite. Casing is usually set at the base of the unconsolidated material (35–45 ft). Static water levels are generally 18–25 ft below ground surface, and rotary mud circulation is the dominant drilling method. Grout is primarily cement, sealing surface to casing depth.